Official Series Description


Lab Data Summary

Aggregate lab data for the FINCH soil series. This aggregation is based on all pedons with a current taxon name of FINCH, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to FINCH were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FINCH soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the FINCH series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the FINCH series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the FINCH series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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There are insufficient data to create the 3D mountains figure.

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Competing Series

Soil series competing with FINCH share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the FINCH series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the FINCH series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

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There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

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Soil series sharing subgroup-level classification with FINCH, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. MI-2010-09-07-10 | Mackinac County - 1997

    Typical pattern of soils and parent material in the Wallace-Spot association (Soil Survey of Mackinac County, Michigan; 1997).

  2. MI-2012-02-06-37 | Mackinac County - 1997

    Typical pattern of soils and parent material in the Wallace-Spot association (Soil Survey of Mackinac County, Michigan; 1997).

Map Units

Map units containing FINCH as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Finch-Kinross complex, 0 to 3 percent slopes252A795614553971kvg9mi00320071:24000
Paquin-Finch sands, 0 to 6 percent slopes160B727914553271kvd1mi00320071:24000
Finch sand, 0 to 3 percent slopes267A118514554091kvgpmi00320071:24000
Spot-Finch complex, 0 to 3 percent slopes266A113214554081kvgnmi00320071:24000
Finch sand, 0 to 3 percent slopes159A5881912546f0hmi00719981:12000
Au Gres-Finch sands, 0 to 4 percent slopesAuA638241488838ymi00919761:15840
Finch sand, 0 to 3 percent slopes49A22181905946db6mi03119881:15840
Finch cobbly sand, 0 to 3 percent slopes141A17981905296d83mi03119881:15840
Finch sand, 0 to 3 percent slopesScA66015881111q9kdmi04119691:24000
Finch sand, 0 to 3 percent slopes159A18741917166fhdmi06919951:15840
Finch-Deford-Au Gres complex, 0 to 3 percent slopes409A18301918556fmwmi06919951:15840
Proper-Finch-Deford complex, 0 to 6 percent slopes410B9231918576fmymi06919951:15840
Finch sand, 0 to 3 percent slopes159A8781906296dcbmi07919981:12000
Spot-Finch complex, 0 to 3 percent slopes89A14918631286p5x2mi09520041:24000
Tawas-Spot-Finch complex, 0 to 3 percent slopes94A8915631296p5xdmi09520041:24000
Paquin-Finch sands, 0 to 6 percent slopes173B5691631318p5y3mi09520041:24000
Finch sand, 0 to 3 percent slopes21A545627469p1xymi09520041:24000
Spot-Finch complex, 0 to 3 percent slopes89A16606416431fzb8mi09719941:20000
Markey-Spot-Finch complex, 0 to 3 percent slopes94A16002416434fzbcmi09719941:20000
Finch-Dawson-Pullup complex, 0 to 35 percent slopes39E7016416399fz97mi09719941:20000
Paquin-Finch sands, 0 to 6 percent slopes173B5929416350fz7nmi09719941:20000
Finch sand, 0 to 3 percent slopes21A3763416377fz8jmi09719941:20000
Paquin-Finch sands, 0 to 5 percent slopes160B3933395106f84cmi10319991:24000
Proper-Finch-Deford complex, 0 to 6 percent slopes410B2831910446dsqmi14319991:12000
Finch sand, 0 to 3 percent slopes159A1661910146drrmi14319991:12000
Spot-Finch complex, 0 to 3 percent slopes26A2898814569541kx2jmi15320071:24000
Rousseau-Neconish-Finch complex, 0 to 25 percent slopes20E952115431671nsslmi15320071:24000
Finch sand, 0 to 3 percent slopes267A507514569531kx2hmi15320071:24000
Paquin-Finch sands, 0 to 6 percent slopes160B429514569211kx1gmi15320071:24000
Au Gres-Finch sands, 0 to 4 percent slopes10A117131907346dgqmi60019831:15840

Map of Series Extent

Approximate geographic distribution of the FINCH soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .